EFFECTS OF COVER CROPPPING ON NITROGEN DIOXIDE, CARBON DIOXIDE AND METHANE FLUXES AND SOIL ENZYME ACTIVITIES IN CORN-SOYBEAN ROTATION SYSTEM

Artemio A. Martin, Jr
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Abstract

The effect of cover crops (ryegrass, hairy vetch, and oilseed radish) in terms of microbial biomass carbon (MBC), C and N mineralization, and enzymatic activities in a corn-wheat-soybean cropping systems under a Mollisol was evaluated. The distributions of total organic C (TOC), total Kjeldahl N (TKN), microbial biomass C (MBC), readily mineralizable C and N, and five enzyme activities (β-glucosidase, β-glucosaminidase, acid phosphatase, arylamidase, and fluorescein diacetate hydrolysis) involved in the cycling of C, N, P and S were studied in three soil depths (0-5. 5-10, 10-20 cm) while soil surface fluxes of carbon dioxide (CO2), methane (CH4), and nitrous oxide (N2O) were estimated. Ryegrass showed higher activity in acid phosphatase, β-glucosidase and β-glucosaminidase. Ryegrass and hairy vetch significantly increased organic C and N, and MBC. Level of mineralized C and N were the same in ryegrass and hairy vetch. There was no clear variation in CO2, N2O and CH4 fluxes from the cover crop treatments. N2O fluxes increased with an increase in soil moisture. The negative CH4 fluxes manifest the soil as CH4 sink. No significant differences among cover crop treatments in terms of CO2-C, N2O-N and CH4-C emissions, a reflection that their emissions are highly variable. Empirical data on carbon dioxide (CO2), methane (CH4) and nitrous oxide (N2O) fluxes are important in management systems to evaluate mitigation strategies, while microbial biomass and enzyme activities can be used as sensitive indicators of ecological stability.
覆盖种植对玉米-大豆轮作系统中二氧化氮、二氧化碳和甲烷通量及土壤酶活性的影响
研究了覆盖作物(黑麦草、毛野豌豆和油籽萝卜)在Mollisol下玉米-小麦-大豆种植体系中微生物生物量碳(MBC)、碳氮矿化和酶活性的影响。研究了总有机C (TOC)、总凯氏定氮(TKN)、微生物生物量C (MBC)、易矿化C和N的分布,以及参与C、N、P、S循环的5种酶活性(β-葡萄糖苷酶、β-葡萄糖苷酶、酸性磷酸酶、芳纶酶和荧光素二乙酸水解)。估算了土壤表面二氧化碳(CO2)、甲烷(CH4)和氧化亚氮(N2O)的通量。黑麦草酸性磷酸酶、β-葡萄糖苷酶和β-葡萄糖苷酶活性较高。黑麦草和毛豌豆显著提高了有机碳、氮和MBC。黑麦草和毛豆的矿化碳和氮水平相同。覆盖作物处理的CO2、N2O和CH4通量变化不明显。N2O通量随土壤湿度的增加而增加。负CH4通量表明土壤为CH4汇。不同覆盖作物处理间CO2-C、N2O-N和CH4-C的排放差异不显著,反映了它们的排放变化很大。二氧化碳(CO2)、甲烷(CH4)和氧化亚氮(N2O)通量的经验数据对管理系统评估缓解策略具有重要意义,而微生物生物量和酶活性可作为生态稳定性的敏感指标。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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